Document Type

Article

Publication Title

Water Resources Research

Publisher

American Geophysical Union.

Publication Date

1-16-2010

Abstract

The sensitivity of snowmelt-driven water supply to climate variability and change is difficult to assess in the mountain west, where strong climatic gradients coupled with complex topography are sampled by sparse ground measurements. We developed a model which ingests daily satellite imagery and meteorological data and is suitable for areas >1000 km2, yet captures spatial variability of snow accumulation and melt in steep mountain terrain.We applied the model for the years 2000–2008 to a 2900 km2 snowmelt-dominated watershed in NW Montana. We found that >25% of the basin’s snow water equivalent (SWE) accumulates above the highest measurement station and >70% accumulates above the mean elevation of surrounding SNOTEL stations. Consequently, scaling point measurements of SWEto describe basin conditions could lead to significant misrepresentation of basin snow. Simulations imply that present-day temperature variability causes measures of snowmelt timing to vary by over 4 weeks from year-to-year. Temperature variability causes a larger spread in snowmelt timing in a warmer climate. On average, snowmelt timing occurs 3 weeks earlier in late 21st century projections, with about 25% of future conditions observed today.

DOI

10.1029/2009WR007861

Comments

An edited version of this paper was published by AGU. Copyright (2010) American Geophysical Union.

Rights

© 2010 by the American Geophysical Union

Recommended Citation

Gillan, B. J., J. T. Harper, and J. N. Moore (2010), Timing of present and future snowmelt from high elevations in northwest Montana, Water Resour. Res., 46, W01507, doi:10.1029/2009WR007861.

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